Soil-archaeological studies of Koy-Gunzhar Scythian tumuli: building materials and technics, diagenetic transformations of buried paleosols
Estudios arqueológicos del suelo de los túmulos escitas de Koy-Gunzhar: materiales y técnicas de construcción, transformaciones diagenéticas de paleosuelos enterrados
Gavrilov D.A. Bronnikova M.A. Khabdulina M.K. Sviridov A.N.
2022Instituto de Geología, Universidad Nacional Autónoma de México
Boletin de la Sociedad Geologica Mexicana
2022#74Issue 3
The tumuli of the Koy-Gunzhar burial ground (2400-2000 cal years BP) in the North Kazakhstan are monumental earthen mounds, built in honour of the Scythian elite. The tumuli, besides representing the diversity of the building techniques for such earth burial mounds, also provide a unique opportunity to study the direction and character of the paleosol diagenesis for nearly 2400 years. This soil-archaeological study aimed to reveal mound building techniques, the characteristics of materials used for construction, and diagenetic changes of the buried paleosols. Comparative analysis of tumulus embankments and buried soils (their genesis and diagenetic transformations) provided the opportunity to establish the source of the building material and to reconstruct some details of the building technologies. For instance, the Calcic Someric Kastanozem (Arenic, Protosodic), buried by loam-sandy and sandy substrate of the tumulus 3 corresponds to dry steppe conditions and has no considerable signs of diagenetic transformations, whereas the paleosol under the tumulus 1 was affected by strong diagenetic transformation supposedly due to acid drainage from the embankment which originally contained sulfidic material being subjected to oxidation and acidification after the tumulus construction. Diagenesis was manifested in the redistribution of pedogenic carbonates and enrichment in iron, magnesium, manganese, and aluminum compounds in the upper 32 cm of the buried soil. These elements were partially accumulated at the carbonate geochemical barrier (over Bk horizon of the buried soil). This soil was transformed by diagenesis from Kasrtanozem to Mollic Cambic Umbrisol (Epiloamic, Katoarenic) The builders of the tumulus 1 used a loamier substrate to construct the mound, different from the parent material for adjacent soils (loamy sands and sands). The loamier substrate ensured the firmness of the mound construction. The builders employed an uncommon technique to produce a mound with defined properties and used foreign building materials brought from the distance.
Building technologies , Diagenesis , Paleosols , Sulfidic material. , Tumuli
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Laboratory of Soil Geography and Genesis, Institute of Soil Science and Agrochemistry, SB RAS, Lavrentieva 8/2, Novosibirsk, 630090, Russian Federation
Department of Soil Geography and Evolution, Institute of Geography, RAS, Staromonetnij 29, Moscow, 119017, Russian Federation
K.A. Akishev Research Institute of Archaeology, L.N. Gumilyov National Eurasian University, Satbaeva 2, Nur-Sultan, 010000, Kazakhstan
Department of Preserving Archaeological Heritage, Institute of Archaeology RAS, Ulyanova 19, Moscow, 117292, Russian Federation
Laboratory of Soil Geography and Genesis
Department of Soil Geography and Evolution
K.A. Akishev Research Institute of Archaeology
Department of Preserving Archaeological Heritage
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